Spectral evolution of wind-generated surface gravity waves in a dispersed ice field

DOI10.1017/S0022112089001096zbMath0666.76050MaRDI QIDQ3817814

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Publication date: 1989

Published in: Journal of Fluid Mechanics (Search for Journal in Brave)

zbMATH Keywords

energy balance equationdispersed ice floesexact nonlinear transfer integralfar-field expressionsFoldy-Twersky integral equationsforced potentialsMarginal Ice ZoneTime-limited wave growthtwo-dimensional discrete spectrum

Mathematics Subject Classification ID

Related Items (9)

Modeling ocean wave propagation under sea ice covers ⋮ Reflection and transmission of regular water waves by a thin, floating plate ⋮ Three-dimensional time-domain scattering of waves in the marginal ice zone ⋮ Attenuation and directional spreading of ocean wave spectra in the marginal ice zone ⋮ Past, present and impendent hydroelastic challenges in the polar and subpolar seas ⋮ A transport equation for flexural-gravity wave propagation under a sea ice cover of variable thickness ⋮ Kinetic equations in a third-generation spectral wave model ⋮ A Semi‐analytic Solution to the Time‐Dependent Half‐Space Linear Boltzmann Equation ⋮ Numerical simulation of the interaction of gravity waves with elastic ice floes

Cites Work

• On the dynamics of unsteady gravity waves of finite amplitude Part 1. The elementary interactions
• On the non-linear energy transfer in a gravity-wave spectrum Part 1. General theory
• Spectral and statistical properties of the equilibrium range in wind-generated gravity waves
• Wave forces on vertical bodies of revolution
• The Motion of Floating Bodies
• On the non-linear energy transfer in a gravity-wave spectrum. Part 3. Evaluation of the energy flux and swell-sea interaction for a Neumann spectrum
• A note on variational principles for surface-wave scattering

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